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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Atmospheric concentrations and deposition of reactive nitrogen in Grand Teton National Park
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Atmospheric concentrations and deposition of reactive nitrogen in Grand Teton National Park

机译:大提顿国家公园的大气浓度和反应性氮的沉积

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The Grand Teton Reactive Nitrogen Deposition Study (GrandTReNDS) was conducted to provide a more complete look at atmospheric concentrations and deposition fluxes of various reactive nitrogen species in and around Grand Teton National Park (GTNP). Daily measurements of wet deposition, PM_(2.5) composition, and gaseous ammonia and nitric acid concentrations were made at three locations. Weekly measurements of gaseous ammonia were made at eight additional sites. Ammonia concentrations were higher at the western sites; the study average ammonia concentration west of GTNP was 35 nmol m~(-3) and on the east side of the park it was 18 nmol m~(-3). Concentrations of other measured reactive nitrogen species were lower than NH_3 and fairly similar at all sites, with averages of approximately 9, 1, and 3 nmol m~(-3) for ammonium, nitrate, and nitric acid, respectively. Wet deposition of ammonium and dry deposition of ammonia were the largest reactive nitrogen deposition pathways, together accounting for 56% and 62% of the nitrogen deposition on the east and west sides of GTNP, respectively. Nitrogen deposition of measured species totaled 2.38 kg N ha~(-1) west of GTNP at Driggs, ID (6 April to 21 September 2011), 0.85 kg N ha~(-1) west of GTNP at a high-elevation site (28 July to 21 September 2011) and 1.23 kg N · ha~(-1) at a location on the east side of GTNP (15 May to 21 September 2011). These measurements highlight the significant inputs of reactive nitrogen to regional ecosystems over the few months studied, the importance of including NH_3 dry deposition in nitrogen deposition budgets, and the need to conduct further research to capture sources and the annual cycle of deposition. Key Points Reactive nitrogen species in Grand Teton National Park Ammonia concentrations were highest to the west of the park Reduced nitrogen contributed the most to total nitrogen deposition
机译:进行了大提顿反应性氮沉积研究(GrandTReNDS),以便更全面地了解大提顿国家公园(GTNP)及其周围地区的大气浓度和各种活性氮物质的沉积通量。每天在三个位置测量湿沉降,PM_(2.5)组成以及气态氨和硝酸浓度。每周在另外八个位置进行气态氨的测量。西部地区的氨气浓度较高。研究表明,GTNP以西的平均氨浓度为35 nmol m〜(-3),在公园的东侧为18 nmol m〜(-3)。其他测得的反应性氮物种的浓度均低于NH_3,并且在所有位点都非常相似,铵,硝酸盐和硝酸的平均值分别约为9、1和3 nmol m〜(-3)。铵的湿沉积和氨的干沉积是最大的反应性氮沉积途径,分别占GTNP东侧和西侧氮沉积的56%和62%。 2011年4月6日至9月21日,内陆地区Driggs的被测物种氮沉降总计为2.38 kg N ha〜(-1),高海拔地区为GTNP以西0.85 kg N ha〜(-1)。 GTNP东侧(2011年5月15日至9月21日)和1.23千克N·ha〜(-1)于2011年7月28日至9月21日)。这些测量结果突出显示了在所研究的几个月中反应性氮对区域生态系统的大量投入,将NH_3干式沉积纳入氮沉积预算中的重要性以及进行进一步研究以捕获源和沉积年循环的必要性。要点大提顿国家公园的活性氮种类氨浓度在公园西边最高,减少的氮对总氮沉积的贡献最大

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